Paleoenvironmental reconstruction in the western lacustrine plain of Llancanelo Lake, Mendoza, Argentina

Lakes are key sites for studying paleoclimates. Llancanelo Lake (southern Mendoza Province, western Argentina) is an endoreic, highly saline water body located in the southern extreme of a tectonic basin, the Central or Huarpes Depression. The lake is located between the Andean Cordillera, San Rafae...

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Autores principales: Violante, R., Osella, A., Vega, M.D.L., Rovere, E., Osterrieth, M.
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_08959811_v29_n3_p650_Violante
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spelling todo:paper_08959811_v29_n3_p650_Violante2023-10-03T15:42:54Z Paleoenvironmental reconstruction in the western lacustrine plain of Llancanelo Lake, Mendoza, Argentina Violante, R. Osella, A. Vega, M.D.L. Rovere, E. Osterrieth, M. Electromagnetic induction methods Geoelectrical soundings Llancanelo Lake Paleoenvironmental reconstruction Volcaniclastic sediments electromagnetic method lake evolution paleoclimate paleoenvironment paleohydrology Quaternary reconstruction vertical electrical sounding volcaniclastic deposit Argentina Llancanelo Mendoza Lakes are key sites for studying paleoclimates. Llancanelo Lake (southern Mendoza Province, western Argentina) is an endoreic, highly saline water body located in the southern extreme of a tectonic basin, the Central or Huarpes Depression. The lake is located between the Andean Cordillera, San Rafael Block and Payenia Volcanic Field. The lake evolved as a major regional depocenter during the Pliocene-Quaternary, hence it contains important thicknesses of intra and extra basinal clastic and evaporitic sediments mainly dominated by volcaniclastic products. The main conditioning factors in the lake evolution were arc and back-arc volcanism as well as climatic changes. Geomorphological and sedimentary evidence supports the hypothesis that the lake was in past times larger than in present days. This paper estimates the lake's former extension on the western lacustrine plain using electromagnetic induction (EMI) and geoelectricity (Multielectrode Resistivity Meter) surveys, as well as shallow wells, along an 8. km long transect perpendicular to the lake's western shoreline. The geophysical and sedimentological information, as well as microfaunal studies, lab analysis and petrographic/EDAX determinations, support the presence, in the subsoil, of a lacustrine sequence at least 30. m thick composed mainly of volcaniclastic sediments. Volcanic eruptions and climatic changes influenced the evolution of the lake, producing intercalations in the lacustrine sedimentary sequences of ash layers, evaporites, soils, and eolian and swamp deposits. © 2009 Elsevier Ltd. Fil:Osella, A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Rovere, E. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_08959811_v29_n3_p650_Violante
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Electromagnetic induction methods
Geoelectrical soundings
Llancanelo Lake
Paleoenvironmental reconstruction
Volcaniclastic sediments
electromagnetic method
lake evolution
paleoclimate
paleoenvironment
paleohydrology
Quaternary
reconstruction
vertical electrical sounding
volcaniclastic deposit
Argentina
Llancanelo
Mendoza
spellingShingle Electromagnetic induction methods
Geoelectrical soundings
Llancanelo Lake
Paleoenvironmental reconstruction
Volcaniclastic sediments
electromagnetic method
lake evolution
paleoclimate
paleoenvironment
paleohydrology
Quaternary
reconstruction
vertical electrical sounding
volcaniclastic deposit
Argentina
Llancanelo
Mendoza
Violante, R.
Osella, A.
Vega, M.D.L.
Rovere, E.
Osterrieth, M.
Paleoenvironmental reconstruction in the western lacustrine plain of Llancanelo Lake, Mendoza, Argentina
topic_facet Electromagnetic induction methods
Geoelectrical soundings
Llancanelo Lake
Paleoenvironmental reconstruction
Volcaniclastic sediments
electromagnetic method
lake evolution
paleoclimate
paleoenvironment
paleohydrology
Quaternary
reconstruction
vertical electrical sounding
volcaniclastic deposit
Argentina
Llancanelo
Mendoza
description Lakes are key sites for studying paleoclimates. Llancanelo Lake (southern Mendoza Province, western Argentina) is an endoreic, highly saline water body located in the southern extreme of a tectonic basin, the Central or Huarpes Depression. The lake is located between the Andean Cordillera, San Rafael Block and Payenia Volcanic Field. The lake evolved as a major regional depocenter during the Pliocene-Quaternary, hence it contains important thicknesses of intra and extra basinal clastic and evaporitic sediments mainly dominated by volcaniclastic products. The main conditioning factors in the lake evolution were arc and back-arc volcanism as well as climatic changes. Geomorphological and sedimentary evidence supports the hypothesis that the lake was in past times larger than in present days. This paper estimates the lake's former extension on the western lacustrine plain using electromagnetic induction (EMI) and geoelectricity (Multielectrode Resistivity Meter) surveys, as well as shallow wells, along an 8. km long transect perpendicular to the lake's western shoreline. The geophysical and sedimentological information, as well as microfaunal studies, lab analysis and petrographic/EDAX determinations, support the presence, in the subsoil, of a lacustrine sequence at least 30. m thick composed mainly of volcaniclastic sediments. Volcanic eruptions and climatic changes influenced the evolution of the lake, producing intercalations in the lacustrine sedimentary sequences of ash layers, evaporites, soils, and eolian and swamp deposits. © 2009 Elsevier Ltd.
format JOUR
author Violante, R.
Osella, A.
Vega, M.D.L.
Rovere, E.
Osterrieth, M.
author_facet Violante, R.
Osella, A.
Vega, M.D.L.
Rovere, E.
Osterrieth, M.
author_sort Violante, R.
title Paleoenvironmental reconstruction in the western lacustrine plain of Llancanelo Lake, Mendoza, Argentina
title_short Paleoenvironmental reconstruction in the western lacustrine plain of Llancanelo Lake, Mendoza, Argentina
title_full Paleoenvironmental reconstruction in the western lacustrine plain of Llancanelo Lake, Mendoza, Argentina
title_fullStr Paleoenvironmental reconstruction in the western lacustrine plain of Llancanelo Lake, Mendoza, Argentina
title_full_unstemmed Paleoenvironmental reconstruction in the western lacustrine plain of Llancanelo Lake, Mendoza, Argentina
title_sort paleoenvironmental reconstruction in the western lacustrine plain of llancanelo lake, mendoza, argentina
url http://hdl.handle.net/20.500.12110/paper_08959811_v29_n3_p650_Violante
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